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El-Gabal El-Ahmar
El-Gabal el-Ahmar ( ar, الجبل الأحمر) is located today within the boundaries of modern-day Cairo, in the area of Nasr City. The name means "The Red Hill". The site was in full production in the times of Akhenaton, Amenhophis III, Tutankhamon and Ramses III. The quarry was directed by Huy also known as "Chief of the King's Works" and also by Hori. The famous Colossi of Memnon are made from blocks of quartzite sandstone probably quarried at El-Gabal el-Ahmar. Typical minerals known from this site: * Celestine, Quartzite Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tect ... or red sandstone. {{Coord, 30.0456113, N, 31.3080056, E, display=title Archaeological sites in Egypt ...
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Cairo
Cairo ( ; ar, القاهرة, al-Qāhirah, ) is the capital of Egypt and its largest city, home to 10 million people. It is also part of the largest urban agglomeration in Africa, the Arab world and the Middle East: The Greater Cairo metropolitan area, with a population of 21.9 million, is the 12th-largest in the world by population. Cairo is associated with ancient Egypt, as the Giza pyramid complex and the ancient cities of Memphis and Heliopolis are located in its geographical area. Located near the Nile Delta, the city first developed as Fustat, a settlement founded after the Muslim conquest of Egypt in 640 next to an existing ancient Roman fortress, Babylon. Under the Fatimid dynasty a new city, ''al-Qāhirah'', was founded nearby in 969. It later superseded Fustat as the main urban centre during the Ayyubid and Mamluk periods (12th–16th centuries). Cairo has long been a centre of the region's political and cultural life, and is titled "the city of a thousand m ...
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Nasr City
Nasr City ( ar, مدينة نصر  ) is a district of Cairo, Egypt. It is located to the east of the Cairo Governorate and consists mostly of condominia. It was established in the 1960s as an extension to neighboring settlement of Heliopolis. The establishment of the district was part of the Egyptian Government's plan to modernise and expand Cairo following the Egyptian Revolution of 1952. Gamal Abdel Nasser, the Egyptian President at the time, was involved personally in the design process, and was the one who chose the name Nasr for the new district ("''nasr''" being the Arabic word for "victory"). During the early stages of the project it was envisioned that it would constitute a new capital city. Now, Nasr City is extremely crowded, much more than was expected from the creation of the district, because of Egyptian families relocating to the district and also because of Somali and South Sudanese immigration to areas of Nasr City such as Hay El Asher (10th Neighbourhood ...
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Akhenaton
Akhenaten (pronounced ), also spelled Echnaton, Akhenaton, ( egy, ꜣḫ-n-jtn ''ʾŪḫə-nə-yātəy'', , meaning "Effective for the Aten"), was an ancient Egyptian pharaoh reigning or 1351–1334 BC, the tenth ruler of the Eighteenth Dynasty. Before the fifth year of his reign, he was known as Amenhotep IV ( egy, jmn-ḥtp, links=no, meaning " Amun is satisfied", Hellenized as ''Amenophis IV''). As a pharaoh, Akhenaten is noted for abandoning Egypt's traditional polytheism and introducing Atenism, or worship centered around Aten. The views of Egyptologists differ as to whether the religious policy was absolutely monotheistic, or whether it was monolatry, syncretistic, or henotheistic. This culture shift away from traditional religion was reversed after his death. Akhenaten's monuments were dismantled and hidden, his statues were destroyed, and his name excluded from lists of rulers compiled by later pharaohs. Traditional religious practice was gradually restored, no ...
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Amenhophis III
Amenhotep III ( egy, jmn-ḥtp(.w), ''Amānəḥūtpū'' , "Amun is Satisfied"; Hellenized as Amenophis III), also known as Amenhotep the Magnificent or Amenhotep the Great, was the ninth pharaoh of the Eighteenth Dynasty. According to different authors, he ruled Egypt from June 1386 to 1349 BC, or from June 1388 BC to December 1351 BC/1350 BC, after his father Thutmose IV died. Amenhotep was Thutmose's son by a minor wife, Mutemwiya. His reign was a period of unprecedented prosperity and splendour, when Egypt reached the peak of its artistic and international power. When he died in the 38th or 39th year of his reign he was succeeded by his son Amenhotep IV, who later changed his name to Akhenaten. Family and early life Amenhotep was the son of Thutmose IV and his minor wife Mutemwiya. He was born probably around 1401 BC. Later in his life, Amenhotep commissioned the depiction of his divine birth to be displayed at Luxor Temple. Amenhotep claimed that his true father was the g ...
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Tutankhamon
Tutankhamun (, egy, twt-ꜥnḫ-jmn), Egyptological pronunciation Tutankhamen () (), sometimes referred to as King Tut, was an Egyptian pharaoh who was the last of his royal family to rule during the end of the Eighteenth Dynasty (ruled in the conventional chronology) during the New Kingdom of Egyptian history. His father is believed to be the pharaoh Akhenaten, identified as the mummy found in the tomb KV55. His mother is his father's sister, identified through DNA testing as an unknown mummy referred to as "The Younger Lady" who was found in KV35. Tutankhamun took the throne at eight or nine years of age under the unprecedented viziership of his eventual successor, Ay, to whom he may have been related. He married his paternal half-sister Ankhesenamun. During their marriage they lost two daughters, one at 5–6 months of pregnancy and the other shortly after birth at full-term. His names—''Tutankhaten'' and ''Tutankhamun''—are thought to mean "Living image of At ...
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Ramses III
Usermaatre Meryamun Ramesses III (also written Ramses and Rameses) was the second Pharaoh of the Twentieth Dynasty in Ancient Egypt. He is thought to have reigned from 26 March 1186 to 15 April 1155 BC and is considered to be the last great monarch of the New Kingdom to wield any substantial authority over Egypt. His long reign saw the decline of Egyptian political and economic power, linked to a series of invasions and internal economic problems that also plagued pharaohs before him. This coincided with a decline in the cultural sphere of Ancient Egypt. However, his successful defense was able to slow down the decline, although it still meant that his successors would have a weaker military. He has also been described as a "warrior Pharaoh" due to his strong military strategies. He led the way by defeating the invaders known as "the Sea Peoples", who had caused destruction in other civilizations and empires. He was able to save Egypt from collapsing at the time when many other em ...
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Colossi Of Memnon
The Colossi of Memnon ( ar, el-Colossat, script=Latn, italic=yes or ''es-Salamat'') are two massive stone statues of the Pharaoh Amenhotep III, which stand at the front of the ruined Mortuary Temple of Amenhotep III, the largest temple in the Theban Necropolis. They have stood since 1350 BC, and were well known to ancient Greeks and Romans, as well as early modern travelers and Egyptologists. The statues contain 107 Roman-era inscriptions in Greek and Latin, dated to between AD 20 and 250; many of these inscriptions on the northernmost statue make reference to the Greek mythological king Memnon, whom the statue was then – erroneously – thought to represent. Scholars have debated how the identification of the northern colossus as "Memnon" is connected to the Greek name for the entire Theban Necropolis as the Memnonium. Description The twin statues depict Amenhotep III ( fl. 14th century BC) in a seated position, his hands resting on his knees and his gaze facing eastwards (a ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ...
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Celestine (mineral)
Celestine (the IMA-accepted name) or celestite is a mineral consisting of strontium sulfate ( Sr S O). The mineral is named for its occasional delicate blue color. Celestine and the carbonate mineral strontianite are the principal sources of the element strontium, commonly used in fireworks and in various metal alloys. Etymology Celestine derives its name from the Latin word ''caelestis'' meaning celestial which in turn is derived from the Latin word ''caelum'' meaning sky or heaven. Occurrence Celestine occurs as crystals, and also in compact massive and fibrous forms. It is mostly found in sedimentary rocks, often associated with the minerals gypsum, anhydrite, and halite. On occasion in some localities, it may also be found with sulfur inclusions. The mineral is found worldwide, usually in small quantities. Pale blue crystal specimens are found in Madagascar. White and orange variants also occurred at Yate, Bristol, UK, where it was extracted for commercial purposes unt ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ...
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